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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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<strong>and</strong> the constant κ is equal to 1 m 1/3 s −1 in SI<br />

units.<br />

manometer A device for measuring pressure<br />

or pressure differences. It consists of a u-shaped<br />

tube, preferably of glass, partially filled with<br />

a liquid (mercury, oil, or water are commonly<br />

used). The difference in height, h, of the liquid<br />

in the two arms of the tube gives the pressure<br />

difference as p =ρgh, where ρ is the fluid<br />

density, <strong>and</strong> g is the local acceleration of gravity.<br />

If the meter-kilogram-second units are used,<br />

the pressure has units of Pascal (Pa). Pressure<br />

difference may also be indicated by givingh <strong>and</strong><br />

the fluid being used, as in “mmHg”, “inches of<br />

Mercury”, “inches of water”.<br />

mantle The terrestrial planets are differentiated<br />

into layers, generally consisting of an outer<br />

crust, interior mantle, <strong>and</strong> central core. The<br />

mantle is usually the largest (by volume) of these<br />

layers <strong>and</strong> is composed of minerals that are intermediate<br />

in density between the iron comprising<br />

the core <strong>and</strong> the lighter materials (such as<br />

feldspars)whichmakeupthecrusts. TheEarth’s<br />

mantle is composed primarily of magnesium,<br />

iron, silicon, <strong>and</strong> oxygen; the mantles of the<br />

other terrestrial planets are believed to be similar.<br />

Seismology indicates that there are several<br />

transition zones within the mantle, the result of<br />

changes in the densities <strong>and</strong> other properties of<br />

the component minerals with depth. Seismic<br />

studies of the Earth’s mantle indicate it is composed<br />

of solid rock, but due to the high temperatures<br />

<strong>and</strong> pressures, the mantle rocks can deform<br />

<strong>and</strong> flow over thous<strong>and</strong>s to millions of years.<br />

This ductile flow of the mantle rocks is called<br />

mantle convection <strong>and</strong> is an efficient process by<br />

which heat is transported from the hot interior of<br />

the Earth to the cooler surface. This convection<br />

is believed to be the driving mechanism for the<br />

platetectonicsoperatingontheEarth. Plumesof<br />

hot material, not necessarily associated with the<br />

mantle convection cells, also occur <strong>and</strong> produce<br />

the hot spots that are responsible for intra-plate<br />

volcanism such as the Hawaiian Isl<strong>and</strong>s.<br />

mantle convection On geologic time scales<br />

theEarth’smantlebehavesasafluidduetosolidstate<br />

creep processes. Because of the heat loss<br />

from the interior of the Earth to its surface, the<br />

© 2001 by CRC Press LLC<br />

March 5th event<br />

deep rocks are hot <strong>and</strong> the shallow rocks are<br />

cool. Because of thermal contraction the cool<br />

near surface rocks are more dense than the hot<br />

deep rocks. This leads to a gravitational instability<br />

with the near surface dense rocks sinking<br />

<strong>and</strong> the deeper light rocks rising. Plate tectonics,<br />

with the subduction of the cool, dense lithosphere,<br />

is one consequence.<br />

mantletransitionzone Azonethatislocated<br />

between depths of 410 <strong>and</strong> 660 km where seismic<br />

velocity <strong>and</strong> density increase markedly with<br />

increasing depth. Sometimes the mantle transition<br />

zone is taken to include the uppermost portion<br />

of the lower mantle down to depths of about<br />

750 to 800 km. Depth distributions of seismic<br />

velocity <strong>and</strong> density, <strong>and</strong> their discontinuities<br />

at depths of 410 <strong>and</strong> 660 km can be explained<br />

by pressure <strong>and</strong> temperature dependency, <strong>and</strong><br />

phase transformations of major composite minerals<br />

(olivine) in pyrolite composition.<br />

March 5th event A gamma ray transient, observed<br />

with 12 spacecraft in 1979, that caused<br />

great controversy. Its properties demonstrated<br />

that it could be a distinct, new class of highenergy<br />

transient. The March 5th event was<br />

clearly identified with the supernova remnant<br />

N49 in the Large Magellanic Cloud (from 55<br />

kiloparsecs away). Its intensity, however, made<br />

it the brightest “gamma ray burst” to date, <strong>and</strong><br />

led many to conclude that its apparent N49<br />

source location must be accidental <strong>and</strong> that it<br />

came instead from a few parsecs away in the<br />

nearby interstellar region, then thought typical<br />

of gamma ray bursts. A few much smaller events<br />

(see soft gamma repeaters) were seen from the<br />

same direction over the years, contrasting to<br />

the apparent lack of repetition of usual gamma<br />

ray bursts, adding to the confusion. Now it is<br />

known, ironically, that gamma ray bursts originate<br />

from cosmological sources, considerably<br />

more distant than even the neighboring galaxies,<br />

<strong>and</strong> that the March 5th event <strong>and</strong> the four known<br />

soft gamma repeaters do originate in “magnetar”<br />

galactic <strong>and</strong> LMC supernova-remnant neutron<br />

stars, including N49. Only one other transient<br />

similar to the March 5th event has been detected<br />

in three decades of space-age monitoring, seen<br />

on August 27, 1998, confirming all aspects of<br />

this interpretation.<br />

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